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地球学报  2002 

断层周围的弹塑性区及其地质意义

Keywords: 断层,非线性本构关系,塑性区,有效应力,屈服应力

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Abstract:

采用弹塑性有限单元方法,通过模拟符合实际状况的逐步加载过程所引起应力场和塑性形变区的研究,得出如下结果:①在塑性或韧性剪切形变情况下,断裂或形变带的共轭剪切角往往大于45°;②在双向挤压应力条件下,先存断裂的前缘部位没有拉伸应力存在,但可能有伸展形变发生;③与最大主压应力夹角为30°~90°的断层前缘是偏应力的优势方位,容易发生塑性剪切形变,特别是夹角为60°左右的断层是最易发生新的构造活动的断层;④多数断层两侧一定范围内以及断层内部是相对的低应力区。这些应力的低值区,非常有利于矿液和油气的运移、聚集和成藏。

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